By Amorin Mello

"Map Showing the Succession of Layers Along Potato River" by R. D. Irving, 1873. Reproduced from the Geology of Wisconsin: Volume III.

“Map Showing the Succession of Layers Along Potato River” by R. D. Irving, 1873. Reproduced from the Geology of Wisconsin: Volume III.

 

opinike0

OPINIKE

(OR POTATOE)

RIVER PROPERTY,

TOWN 46, NORTH RANGE 1, WEST, SECTIONS 16 & 17,

480 ACRES,

ASHLAND COUNTY, WISCONSIN.

————–

Detail of Township 45 North, Range 1 West, from Charles Whittlesey’s 1860 Geological Map of the Penokie Range.

Detail of the Opinike River Property and the Ironton trail in Township 45 North, Range 1 West, from Charles Whittlesey’s 1860 Geological Map of the Penokie Range.

The “Charter Oak” Mining Company occupied these premises in 1845-6 under permits from the government. The reports of the agents of the Company at that time state that copper bearing veins were found in the trap rocks next above the lower Falls. In geological characters and position, the rocks are the same here as at the Upper Falls of the Montreal, herein described. Next below the sandstone is the same black slate; below this the conglomerate, then alternating bands of sandstone and trap, and beneath them the main body of brown and amygdaloid trap. Like the Montreal River beds, they are here tilted up at a high angle to the North-west, their line of outcrop bearing North-east. They are, however, reduced in thickness materially, the conglomerate being about 600 feet, and the bands f sandstone are fewer in number. over the conglomerates, and over the trap, there are several falls and chutes in the river, amounting to 125 or 130 feet in a mile.

Detail of the Upper Falls (Saxon Falls) on the Montreal River in Township 47 North, Range 1 East from Charles Whittlesey’s 1860 Geological Map of the Penokie Range.

Detail of the Upper Falls (Saxon Falls) on the Montreal River and the Old Flambeau Trail in Township 47 North, Range 1 East from Charles Whittlesey’s 1860 Geological Map of the Penokie Range.

Here, as at the Montreal, the best trap is above the chutes, where it is well exposed in the channel of the river. For one mile above the Lower Falls the trap is of a favorable character ; but above this is not visible until the old Ironton trail is reached. The thickness of the productive trap is not as great as it is at the Montreal River. I judge that this tract covers the entire breadth of the soft brown amygdaloid trap. So far as I can form an opinion from the eternal character of the rocks, they promise as well as any part of this range. No part of the ground has been tested by recent explorations for veins, but there is abundant encouragement for a thorough trial. It must be remembered that it is only in the streams that the rocks composting the best part of this copper range are visible. From the Montreal to the Opinike River, neither the conglomerate nor the trap rises above the level of the country. From the Opinike to the forks of Bad River on Section 17, Town 45, Range 2, West, a distance South-easterly of about nine (9) miles, the productive belt of trap does not show itself above the drift materials, which over the country. The process of exploration is therefore much more tedious than it would be if the uplift was elevated into a high mountain ridge, with rocky cliffs exposed to view.

Ironton townsite claim at Saxon Harbor with trails to Odanah and the Penoka Iron Range. (Detail from Wisconsin Public Land Survey Records during November of 1861)

Detail of Ironton landing and trail from T47N R1W.

Ironton is the proper landing for works at the Opinike Falls, as well as for the Montreal River, and the distance is about nine miles. About two miles up the river, the Ironton trail to the Iron Range, crosses the River Opinike. It is highly probable the Ashland Copper Mining Company, which is now at work at the forks of Bad River, will seek an outlet this way. Although there is not a natural harbor at Ironton Landing, there is an angle in the cast which gives shelter to all but Northern winds, and the deep water approaches near the shore. Piers that were sunk there in 1857, have not yet been moved from their foundations by storms or by floating ice. This is the natural outlet for that part of the Iron Range which is East of the Penokie Gap. Although the country is somewhat mountainous, there are no serious obstacles to prevent highways, plank-roads or railroads from being built. Whatever mines may be developed on either the Copper or the Iron Range East of the Bad River, will find this the most convenient route to reach the lake. The water-power of the Opinike is at the upper chutes twenty-eight (28) feet and the lower seventy-five (75) feet – the latter being over the conglomerate rock and the former over trap. It is about three-fourths of a mile between them, and in the distance the river is rapid over a rocky bed. There is sufficient timber on the tract for all mining purposes, and a portion of the soil is equal to any in the country.

From the falls of the Opinike to Lehy’s saw-mill, at the falls of Bad River, is about nine (9) miles, in a North-westerly direction. Batteaux can reach Lehy’s mill from the lake during the ordinary stage of water. There is an Indian trail from Lehy’s to the falls, over a level country, somewhat more feasible for a road than the route to Ironton, but for the purposes of a mine the Ironton landing is much preferable. The flow of water in the Opinike is not equal to that of the Montreal, but the total fall is greater. Should workable mineral be found here – as appearances lead me confidently to anticipate – the location has advantages of position and water-power such as to place it next the Montreal River property for economical mining.

CHAS. WHITTLESEY,

Geologist and Mining Engineer.

Cleveland, Jan’y 1st, 1865.

By Amorin Mello

Map and Section Showing the Formations at the Junction of Bad River and Tylers Fork" by R. D. Irving, 1873. Published in the Geology of Wisconsin: Volume III.

“Map and Section Showing the Formations at the Junction of Bad River and Tylers Fork” by R. D. Irving, 1873. Reproduced from the Geology of Wisconsin: Volume III.

 

LETTER OF J. A. BAILEY, ESQ.,

IN REFERENCE TO THE

TYLER’S FORK PROPERTY.

———–

Office of Ashland Copper Mining Company,
Ashland County, Wis., Oct. 20, 1864.

Messrs. A. Whittlesey F. W. Bartlett,

Gentlemen:

"Asaph Whittlesey dressed for his journey from Ashland to Madison, Wisconsin, to take up his seat in the state legislature. Whittlesey is attired for the long trek in winter gear including goggles, a walking staff, and snowshoes." Circa 1860. ~ Wisconsin Historical Society

Asaph Whittlesey dressed for his journey from Ashland to Madison, Wisconsin, to take up his seat in the state legislature. Whittlesey is attired for the long trek in winter gear including goggles, a walking staff, and snowshoes.” Circa 1860.
~ Wisconsin Historical Society

I have made an examination of the trap beds exposed between this and your location, upon the Copper Range, in Sections 15, 16 and 21, Town 45, North, Range 2, West, in this County, and have collected specimens (which are herewith forwarded) from the Ashland Company’s location, and from various points Eastward to your location.

The accompanying sketch of the territory referred to will assist you in locating the several points from which these specimens were taken, the figures upon the sketch indicating the points referred to.

Detail of the Ashland Copper Mine from 1873; now Copper Falls State Park.

Detail of the Ashland Copper Mine from 1873; located around what is now the main picnic area within Copper Falls State Park.

The specimens No. 1, are from the rocks in place in the bed of the West branch of Bad River, above the falls, near shaft No. 1, and contain a good per centage of native Copper. The copper bearing belt, exposed here across the formation, embraces a breadth of about 500 feet.

Specimens No. 2, are vein rock, from the transverse vein, in which our shaft No. 1 is being sunk. This shaft is now 35 feet deep, carrying small quantities of fine Copper all the way.

The Herbert vein was named after William Herbert: former copper mining agent for the American Fur Company; and former iron mining agent for the Wisconsin & Lake Superior Mining & Smelting Company.

Specimens No. 3, are from the outcrop of the Herbert vein, near the junction of the East and West branches of Bad River, containing “gray ore,” or “gray sulphuret of copper.”

Specimens Nos. 4, 5 and 6 are of trap, taken from the rock in place, along Tyler’s Fork, at the points indicated on the sketch of corresponding numbers.

My explorations and survey have been extended only to a short distance East of the Section line dividing Sections 16 and 17.

The surveys have been carefully made with theodolite and chain, with the view to determine the true course of the copper bearing belt through the “Ashland Company’s” property, and that adjoining on the East; and as near as I can determine from the measurements and the character of the rocks exposed, the course of this belt is East and West, or nearly so, through Section 17, with indications of a curve to the Northward, as we approach to, and enter Section 16.

I have indicated on the sketch the position of what I consider the North line of the outcrop of the copper bearing belt. The South line is not determined, the rocks being covered by drift, sand, &c.

It will be proper for me to add that the productive trap formation, found in place above the falls, in the West branch, corresponds fully with the formation at the same elevation in Tyler’s Fork, on the Western boundary of Section 16; and I am clearly of the opinion that at that point the trap formation, when penetrated to a depth corresponding to that at the falls of the West branch, will be alike productive of copper, and that the most productive veins will be found running parallel with the formation.

Very respectfully, Yours, &c.,

J. A. BAILEY,

Supt. & Engineer A. C. M. Co.

—————-

Ervin “Nigigoons” Leihy had a sawmill located at the Falls on Bad River.

A letter from Mr. E. Leehy, of Bad River Falls, dated Jan’y 6, 1865, states that in shaft No. 2, on the Ashland mine, several hundred feet South of No. 1, and in the productive belt, the copper rock was reached at 20 feet in depth, and the first blast threw out several pounds of native copper in pieces from the size of an egg down.


 

tylersforklocation1

“Property on which ‘Silver Lead’ has recently been discovered.”

TYLER’S FORK LOCATION.

——-~~0~~——-

COPPER LANDS,

IN
SECTIONS 15 16 AND 21, TOWN 45, NORTH, RANGE 2, WEST.

640 ACRES.

ASHLAND COUNTY, WISCONSIN.

Detail of Township 45 North, Range 2 West, from Charles Whittlesey's 1860 Geological Map of the Penokie Range.

Detail of Township 45 North, Range 2 West, from Charles Whittlesey’s 1860 Geological Map of the Penokie Range.

This location covers a great part, if not all of the breadth of the productive trap formation. The outcrop of the strata is here nearly East and West, with a curve to the North-Eastward on or near this land. The greatest length of the location is North and South, and therefore crosses the formation nearly at right angles. At the Northern end, is the conglomerate and sand rock, which overlies the trap beds. These beds are better exposed at the West, in Section 17, on the Ashland Copper Company’s land, where they are now working and whatever developments may be made there will apply to this property. The strata have a sharp dip to the North, and are thus exposed at the edges, being nearly vertical. Next below, and South of the conglomerate, is a band of black and red trap, of a compact and rather flinty structure, about three hundred (300) feet thick, in which there are numerous transverse veins, cutting the strata at various angles. These are visible in a deep gulf formed on both forks of Bad River, that unite in Section 17. Somme of these cross veins carry copper, both native and as an ore in the form of grey sulphuret. They also carry as vein matter, chlorite, cale, spar, and flucan, or red and green magnesian clay. There are also narrow beds of trap, interstratified with the hard ores, which are softer, owing to a large portion of laumonite. I do not regard the true veins in the upper beds, as likely to furnish mining ground; but as highly valuable indications, which are to be followed into the more promising strata lower down in the system. Next below the hard beds, to the South, is a belt of trap rocks, whose composition and texture I regard as highly favorable.

The Ashland Company is sinking on a cross or transverse vein, at the Southern border of the hard beds; which in the course of 75 or 100 feet along their inclined shaft, will enter what I consider productive ground. The thickness of this ground is not determined, but what I have seen in the branches of the river exceeds half a mile. It is not, however, all alike, as there are in it layers possessing different characters, corresponding in this respect other parts of the trap range in Michigan and Wisconsin.

The stratum at the head of the falls, on the West fork, where the Ashland Company is at work, has been closely examined over a breadth of about 50 feet, and carries small pieces or nuggets of native copper throughout. It is a soft brown amyglaloid, which small bunches of chlorite, spar and laumonite; some prehnite and quartz, in which the copper is found. Lumps weighing one to two pounds have been obtained from this bed away from any appearances of a vein. This is the general character of the mineral belt on Section 17, which I consider as the true mining ground of this part of the range. All these beds are embraced in our location, at a distance of ¼ to ⅓ of a mile on the East. In Sections 16 and 21, the exposure of rock is not as extensive as it is upon 17, for the rocks are covered by drift clay, sand and gravel, except in the streams.

“The most easterly of the two middle forks I have called ‘Tyler’s Fork,’ which is divided above its falls into two equal branches; the other, which preserves the general direction of the main trunk, may, with propriety, retain its name, as the Mashkeg or Bad River.
There is no canoe navigation on Tyler’s Fork, or the Upper Bad River, so swift is the current and narrow and crooked are the channels.
Tyler’s Fork comes out of the mountains about twelve miles southeast by south from Woods’s [at Leihy’s Saw Mill], in a chasm, two hundred feet deep deep, in the red sand-rock and conglomerate. The junction of its ten branches takes place in this narrow gulf or ‘cañon,’ the eastern branch making a plunge of forty-two feet, succeeded, as you ascend, by a series of chutes over trap-rocks forty feet in one-fourth of a mile. Mr. D. Tyler, of the Charter Oak Company, made a location here, and built a rude cabin at the edge of the falls.”
Geological Report on That Portion of Wisconsin Bordering on the South Shore of Lake Superior.  Surveyed in the Year 1849, Under the Direction of David Dale Owen, United States Geologist, by Charles Whittlesey, Head of Sub-Corps, page 433.
"Studio portrait of geologist Charles Whittlesey dressed for a field trip." Circa 1858. ~ Wisconsin Historical Society

“Studio portrait of geologist Charles Whittlesey dressed for a field trip.” Circa 1858.
~ Wisconsin Historical Society

The East, or “Tyler’s” Fork, shows the trap beds in its channel a large part of the way through Section 16; and they are visible in the small creek that empties into it on Section 21, from the South. To examine the metal-bearing bed, of which I have spoken, after it reaches this location, the rocks must be uncovered by trenches or shafts in the sand and gravel, after having determined the true course of the bed. The search for cross veins can be easily made in the channel of Tyler’s Fork. This is a stream of considerable value for water power, the fall in your property being sufficient for two dams, and the flow of water sufficient for a saw mill. The Exploration of the porous laumonite beds, will be somewhat tedious; but the close proximity to those on the Ashland Company’s property will be of great assistance. As soon as it is demonstrated that these deposits of fine and nugget copper are remunerative at one point on the range, it gives new value to the whole system. Copper deposited in this mode, in other mining districts, has been found to be more uniform over long distances, than it is in veins; because these ores are liable to pass out of the property formations, and into a diabase rock. These copper-bearing longitudinal courses should therefore be most thoroughly searched. In this region, stamp mills can be worked in most cases by water power; a heavy and regular bed can be stoped and broken up ready for the mill, at a much cheaper rate per fathom, than vein matter. The improved stamps, crushers and washers, have of late years much reduced the expence of working mineral-bearing rock. The absence of masses of native copper in the Ashland district, is not now so important as it was when the first explorers made their location here. On this property, the length of the copper-bearing beds is something over a mile, and their breadth at least half a mile. As they extend to a greater depth than any mine can be worked, there is no fear of exhaustion.

CHAS. WHITTLESEY

Geologist and Mining Engineer.

Cleveland, Ohio, Jan. 1st, 1865.

By Leo

“The Usual Irish Way of Doing Things”, by Thomas Nast Published 2 September 1871 in Harper’s Weekly.  Nast, who battled Tammany Hall and designed the modern image of Santa Claus, is one of the most famous American political cartoonists.  However, he frequently depicted Irish-Americans as drunken, monkey-like monsters (Wikimedia Images).

It has been a while since I’ve posted anything new.  My personal life has made it impossible to meet my former quota of three new posts a month.  Now, it seems like I’ll be lucky to get one every three months.  I haven’t forgotten about this site, however, and there is certainly no shortage of new topics.  Unfortunately, most of them require more effort than I am able to give right now.  Today, however, I have a short one.

Regular readers will know that the 1855 La Pointe annuity payment to the Lake Superior Chippewa bands is a frequent subject on Chequamegon History.  To fully understand the context of this post, I recommend reading some of the earlier posts on that topic.  The 1855 payment produced dozens of interesting stories and anecdotes:  some funny, some tragic, some heroic, some bizarre, and many complicated.  We’ve covered everything from Chief Buffalo’s death, to Hanging Cloud the female warrior, to Chief Blackbird’s great speech, to the random arrival of several politicians, celebrities, and dignitaries on Madeline Island.   

Racism is an unavoidable subject in nearly all of these stories.  The decisive implementation of American power on the Chequamegon Region in the 1850s cannot be understood without harshly examining the new racial order that it brought.  

The earlier racial order (Native, Mix-blood, European) allowed Michel Cadotte Jr., being only of one-eighth European ancestry to be French while Antoine Gendron, of full French ancestry, was seen as fully Ojibwe.  The new American order, however, increasingly defined ones race according to the shade of his or her skin.

But there are never any easy narratives in the history of this area, and much can be missed if the story of American domination is only understood as strictly an Indian/White conflict.  There are always misfits, and this area was full of them.  

I recently found an example from the November 7, 1855 edition of the Western Reserve Chronicle in Warren, Ohio shows just how the suffocating paternalism  directed toward the Ojibwe at the 1855 payment hit others as well: 

A GENUINE IRISHMAN

A correspondent of the Home Journal relates the following characteristic incident of Irish tactic.  He says:

Does the wide world contain another paradox that will compare with a real bona fide, unmitigated Irishman?  Imagination and sensuality, poetry and cupidity, generosity and avarice, heroism and cowardice–and so on, to the end of the list; all colors, shades and degrees of character congregated together, and each in most intimate association with its intensest antithesis–a very Joseph’s coat, and yet, most marvelous of marvels! a perfect harmony pervading the whole.

Among the reminiscences of a month’s sojourn at La Pointe, Lake Superior, during the annual Indian payment of the last summer, I find the following truly ‘representative’ anecdote:

One day while Commissioner Monypenny was sitting in council with the chiefs, intelligence was brought to Mr. Gilbert (the Indian agent) that two or three Indians were drunk and fighting, at a certain wigwam.  With his usual promptitude, Mr. Gilbert summoned one of his interpreters, and proceeded directly to the lodge, where he seized the parties and locked them in the little wooden jail of the village, having first ascertained from them where they obtained their liquor.  He then went immediately to the house they had designated, which was a private dwelling, occupied by an Irishman and his wife, and demanded if they kept liquor to sell to the Indians.

Henry C. Gilbert was the Indian Agent during the Treaty of 1854 and oversaw the 1855 annuity payment along with Commissioner of Indian Affairs George Manypenny (Branch County Photographs).

Both the man and woman, with rational vehemence and volubility–and both at once, of course, utterly denied having ‘a dhrop in the house, more nor a little jug full, which we just kape by us, like, for saysonin’ the vittals, and sickness.’  But, unfortunately for the veracity of the parties, on searching the premises, the interpreter discovered, in a little back wood-shed, two barrels of whiskey, besides the ‘little jug’ which proved to be a two gallon one, and full.

Mr. Gilbert ordered some of his men to roll the barrels out on the green, where in the presence of the whole council, they knocked in head, and the jug broken.  But the flow of whisky was as nothing compared with the Irish wife’s temper, meanwhile.  I had never conceived it possible for a tongue to possess such leverage; it seemed literally to be ‘hung in the middle and to work both ways.’  However, mother Earth drank the whisky, and the abuse melted into ‘the circumambient air’–though one would not have suspected their volubility, they seemed to be such concrete masses of venom.

In the evening of the same day, as Col. Monypenny was walking out with a friend, he encountered and was accosted by, the Irish whisky vender.

‘The first star of the avenin’ to yees, Misther Commissioner!  An’ sure it was a bad thrick ye were putting on a poor mon, this mornin’.  Och, murther!  to think how ye dissipayted the illegant whisky; but ye’ll not be doin’ less nor payin’ me the first cost of it, will ye?’

‘On the contrary,’ said the commissioner, ‘we are thinking of having you up in the morning, and fining you; and if we catch you selling another drop to the Indians, we shall forcibly remove you from the island.’

Quick as–but I despair of a simile, for surely there is no operation of nature or art that will furnish a parallel to the agility of an Irishman’s wit–his whole tone and manner changed, and dropping his voice to the pitch confidential, he said:

‘Wll, Misther Commissioner, an’ its truth I’m tellin’ ye–its mighty glad I was, intirely, to see the dirty barrels beheaded; sure I’d a done it meself, for the moral of the thing, ef it hadn’t been for the ould woman.  Good avenin’ to ye, Misther Commissioner.’

It is hardly necessary to add that no further application was made for the ‘first cost of it.’

Very truly yours.

~ Western Reserve chronicle. (Warren, Ohio) November 07, 1855

(Library of Congress Chronicling America Historic Newspaper Collection)

The sale of alcohol was illegal at La Pointe at that time.  However, the law was generally impossible to enforce and liquor flowed freely into and out of the island.

Admittedly I chuckled at the depiction of the Irish wit and the temper of the “Irish wife,” but as a descendant of immigrants who fled the Great Famine in the 1840s, it’s hard to read the condescending stereotypes my ancestors would have been subjected to.  

That said, it’s important to note that the two or three Ojibwe people in this story were imprisoned without charges or trial for drinking, while the couple selling the illegal liquor only lost his stock and wasn’t fined.  This is something those of us of European descent need to be careful of when trying to draw equivalencies.

So then who was the bona fide, unmitigated Irishman?

Hundreds of thousands of Irish immigrants came to America during the 1840s and ’50s.  Inevitably, some of them ended up in this area.  However, by 1855 it was only a handful.  

Just a few weeks prior to the payment, Alexis Carpentier, a former voyageur from a mixed French-Ojibwe family was charged with taking the Wisconsin State Census for La Pointe County.  He found 37 residents of foreign birth.  Most of these were French or mix-blooded men, born in Canada, who married into local Ojibwe and mix-blood families.  

In only one household, more than one person is listed as being foreign-born.  This was the home of Patric Sullivan.  State censuses only listed the name of the head of household and do not list country of origin.  However, in the 1860 Federal census, we find Patrick and Johanna Sullivan living with their three sons in La Pointe township.  Both were born in Ireland.

Page 1 of 1855 Wisconsin State Census for La Pointe County (familysearch.org)

Pages 2 and 3. Patric Sullivan is fourth from the bottom on the right side. enlarge

Pages 4 and 5.

Page 6 with totals.

Patrick Sullivan did not sign the LaPoint Agreement to Stop Whiskey Trade of September 10, 1855. In fact, I haven’t been able to find much information at all about Patrick and Johanna Sullivan in later years.  It does appear the family stayed in the area and their children were still living in Ashland at the dawn of the 20th century.

Finally, since this post deals with the 1855 census and issues of race and identity, it’s worth noting another interesting fact.  The state census had only two categories for race:  “White” and “Colored.”  As non-citizens, full-blooded Ojibwe people would not have been counted among the 447 names on the census.  However, it seems that Carpentier and his boss, La Pointe town clerk Samuel S. Vaughn, were not sure how to categorize by race.  

Carpentier crossed out the designation “Colored” and replaced it with “Half-Breed.”  By their count, 329 “Half-Breeds” and 118 Whites (many of them in mixed families) lived in La Pointe County in 1855.  Mix-bloods were considered Ojibwe tribal members under the Treaty of 1847.  However, they traditionally had their own identity and were thought eligible for U.S. citizenship.  

One wonders what conversations were had as the census was completed, but in the final compilation, all 447 names (including several core Red Cliff and Bad River families) were submitted to the state as “White” rather than “Colored.”  Despite America’s best efforts to create a racial duality, which would only intensify following the Civil War, this region would continue to defy such categorization for the remainder of the 19th century.

Sources:
Kohl, J. G. Kitchi-Gami: Life among the Lake Superior Ojibway. St. Paul: Minnesota Historical Society, 1985. Print.
Miller, Kerby A. Emigrants and Exiles: Ireland and the Irish Exodus to North America. New York: Oxford UP, 1985. Print.

NOTES:  Research originally featured on Chequamegon History is featured in the new Changing Currents exhibit opening today at the Chippewa Valley Museum in Eau Claire.  I had a chance to preview the exhibit on Friday, and John Vanek and crew have created an incredibly well-done display of Ojibwe treaty and removal politics of the mid 1800s.  See their website for more information.  The research found in this exhibit, which extends into several topics, is very deep and does not shy away from uncomfortable topics.  I highly recommend it.

There may be some exciting guest research featured on Chequamegon History in the coming months dealing with the aftermath of the 1854 Treaty and fraudulent land claims in the Penokee Iron Range.  Stay tuned.